Aerosol optical properties and its radiative forcing over Yulin, China in 2001 and 2002

被引:31
作者
Che Huizheng [1 ]
Zhang Xiaoye [1 ]
Alfraro, Stephane [2 ]
Chatenet, Bernadette [2 ]
Gomes, Laurent [3 ]
Zhao Jianqi [4 ]
机构
[1] Chinese Acad Meteorol Sci, China Meteorol Adm, Ctr Atmosphere Watch & Serv, Key Lab Atmospher Chem, Beijing 100081, Peoples R China
[2] Univ Paris VII Paris XII, Lab Interuniv Syst Atmosph, F-94010 Creteil, France
[3] Meteo France CNRM GMEI MNPCA, CNRS, F-31057 Toulouse, France
[4] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
aerosol optical properties; aerosol radiative forcing; Mu Us desert; China; MINERAL AEROSOL; CLIMATE-CHANGE; DESERT DUST; ACE-ASIA; AERONET; TRANSPORT; REGION; SUN; SCATTERING; SATELLITE;
D O I
10.1007/s00376-009-0564-4
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The aerosol optical properties and direct radiative forcing over the Mu Us desert of northern China, acquired through a CE318 sunphotometer of the ground-based Aerosol Robotic Network (AERONET), are analyzed. The seasonal variations in the aerosol optical properties are examined. The effect of meteorological elements (pressure, temperature, water vapor pressure, relative humidity and wind speed) on the aerosol optical properties is also studied. Then, the sources and optical properties under two different cases, a dust event and a pollution event, are compared. The results show that the high aerosol optical depth (AOD) found in Yulin was mostly attributed to the occurrence of dust events in spring from the Mu Us desert and deserts of West China and Mongolia, as well as the impacts of anthropogenic pollutant particles from the middle part of China in the other seasons. The seasonal variation and the probability distribution of the radiative forcing and the radiative forcing efficiency at the surface and the top of the atmosphere are analyzed and regressed using the linear and Gaussian regression methods.
引用
收藏
页码:564 / 576
页数:13
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